[1] Hanson A D, Zhang S C, Moldowan J M, et al. Molecular organic geo chemistry of the Tarim basin,Northwest China. AAPG Bulletin, 2000, 84(8): 1109～1128
[2] Cheng J, Fu J, Sheng G, et al. Diamond hydrocarbon ratios:novel maturity indices for highly mature crude oils. Organic Geochemistry,1996, 25(3/4): 179～190
[3] Zhang S, Moldowan J M, Bian L, et al. Biological and molecualr geochemical evidence for dinoflagellate ancestors in the Upper Sinian-Cambrian. Acta Geologica Sinica, 2000, 74(4):740～747
[4] Zhang S, Hanson A D, Moldowan J M, et al. Paleozoic oil-source rock correlations in the Tarim basin,NW China. Organic Geochemistry, 2000, 31(4): 273～286
[5] 黄第藩,赵孟军. 下古生界海相原油之中蜡的成因分析--干酪根PY-GC分析提供的证据. 沉积学报,1996, 14(2):12～19[Huang D, Zhao M. The genesis of marine oils with middle wax from Lower Palaeozoic--evidences obtainined from kerogens PY-GC analysis. Acta Sedimentologica Sinica, 1996, 14(2):12～19]
[6] Wilhelms A, Telnaes N, Steen A, et al. A quantitative study of aromatic hydrocarbons in a natural maturity shale sequence-the 3-methylphenanthrene/retene ratio,a pragmatic maturity parameter. Organic Geochemistry, 1998, 29(1～3): 97～105
[7] 刘德汉,史继扬, 郑旭明. 高演化碳酸盐岩的地球化学特征及非常规评价方法的探讨.天然气工业,1994,14(增刊): 62～66[Liu D, Shi J, Zheng X. A discussion on the geochemical characteristics and unconventional evaluation method of high altered carbonate rocks. Natural Gas Industry, 1994, 14(suppl.): 62～66]
[8] Fan P, Philp R P, Li Z, et al. Geochemical characteristics of aromatic hydrocarbons in crude oils and source rocks from different sedimentary environments. Organic Geochemistry, 1990, 16(1～3): 427～435